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dc.contributor.authorGarcía Díez, Markel 
dc.contributor.authorFernández Fernández, Jesús (matemático) 
dc.contributor.authorVautard, Robert
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2016-12-21T13:46:03Z
dc.date.available2016-12-21T13:46:03Z
dc.date.issued2015-12
dc.identifier.issn0930-7575
dc.identifier.issn1432-0894
dc.identifier.otherCGL2010-22158-C02es_ES
dc.identifier.otherCGL2010-21869es_ES
dc.identifier.otherCGL2011-28864es_ES
dc.identifier.urihttp://hdl.handle.net/10902/9842
dc.description.abstractRegional Climate Models (RCMs) are widely used tools to add detail to the coarse resolution of global simulations. However, these are known to be affected by biases. Usually, published model evaluations use a reduced number of variables, frequently precipitation and temperature. Due to the complexity of the models, this may not be enough to assess their physical realism (e.g. to enable a fair comparison when weighting ensemble members). Furthermore, looking at only a few variables makes difficult to trace model errors. Thus, in many previous studies, these biases are de- scribed but their underlying causes and mechanisms are often left unknown. In this work the ability of a multi-physics ensemble in reproducing the observed climatologies of any variables over Europe is analysed. These are temperature, precipitation, cloud cover, ra- diative fluxes and total soil moisture content. It is found that, during winter, the model suffers a significant cold bias over snow covered regions. This is shown to be re- lated with a poor representation of the snow-atmosphere interaction, and is amplified by an albedo feedback. It is shown how two members of the ensemble are able to alleviate this bias, but by generating a too large cloud cover. During summer, a large sensitivity to the cumulus parameterization is found, related to large differences in the cloud cover and short wave radiation flux. Results also show that small errors in one variable are sometimes a result of error compensation, so the high dimensionality of the model evaluation problem cannot be disregarded.es_ES
dc.description.sponsorshipThis work was partially supported by Projects EXTREMBLES (CGL2010-21869) and CORWES (CGL2010-22158-C02), funded by the Spanish R&D Programme. WRF4G (CGL2011-28864) provided the framework to run the model; this Spanish R&D project is co-funded by the European Regional Development Fund (ERDF). Partial support from the 7th European Framework Programme (FP7) through Grant 308291 (EUPORIAS) is also acknowledged.es_ES
dc.format.extent17es_ES
dc.language.isoenges_ES
dc.publisherSpringeres_ES
dc.rights© Springer. This version of the article has been accepted for publication, after peer review (when applicable) and is subject to Springer Nature's AM terms of use, but is not the Version of Record and does not reflect post-acceptance improvements, or any corrections. The Version of Record is available online at: https://doi.org/10.1007/s00382-015-2529-xes_ES
dc.sourceClimate Dynamics, 2015, 45(11-12), 3141-3156es_ES
dc.subject.otherWRFes_ES
dc.subject.otherCERESes_ES
dc.subject.otherE-OBSes_ES
dc.subject.otherGLDASes_ES
dc.subject.otherCORDEXes_ES
dc.subject.otherEURO-CORDEXes_ES
dc.subject.otherMulti-physicses_ES
dc.subject.otherModel evaluationes_ES
dc.subject.otherRadiationes_ES
dc.subject.otherSoil moisturees_ES
dc.titleAn RCM multi-physics ensemble over Europe: Multi-variable evaluation to avoid error compensationes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttps://doi.org/10.1007/s00382-015-2529-xes_ES
dc.rights.accessRightsopenAccesses_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/FP7/308291/EU/EUropean Provision Of Regional Impact Assessment on a Seasonal-to-decadal timescale/EUPORIAS/es_ES
dc.identifier.DOI10.1007/s00382-015-2529-x
dc.type.versionacceptedVersiones_ES


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